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Decadal Trend of Dust Activities in Middle East Shifts from Positive to Negative around 2010

Decadal Trend of Dust Activities in Middle East Shifts from Positive to Negative around 2010
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Study attributes shift of decadal trend in Middle East dust activities to North Tropical Atlantic variability

Study attributes shift of decadal trend in Middle East dust activities to North Tropical Atlantic variability
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Frontiers | Toward Understanding El Niño Southern-Oscillation's Spatiotemporal Pattern Diversity

The El Niño Southern Oscillation (ENSO) phenomenon, manifested by the great swings of large-scale sea surface temperature (SST) anomalies over the equatorial central to eastern Pacific oceans, is a major source of interannual global shifts of climate patterns and weather activities. ENSO's SST anomalies exhibit remarkable spatiotemporal pattern diversity (STPD), with their spatial pattern diversity dominated by Central Pacific (CP) and Eastern Pacific (EP) El Niño events and their temporal diversity marked by different timescales and intermittency in these types of events. By affecting various Earth system components, ENSO and its STPD yield significant environmental, ecological, economic, and societal impacts over the globe. The basic dynamics of ENSO as a canonical oscillator generated by coupled ocean-atmosphere interactions in the tropical Pacific have been largely understood. A minimal simple conceptual model such as the recharge oscillator paradigm provides means fo

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Increase in North Tropical Atlantic Variability with Warming Climate

Increase in North Tropical Atlantic Variability with Warming Climate
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